GLAUCODOTE Meaning and
Definition
-
Glaucodote is a mineral compound belonging to the arsenic sulfides group. It is classified as a sulfarsenide, with its chemical composition primarily consisting of arsenic and sulfur. The general formula for glaucodote is (Cu^+,Ag^+)AsS. It is commonly found as submetallic, bluish-gray to black-colored crystalline aggregates.
Glaucodote typically occurs in hydrothermal deposits, where it forms as a secondary mineral associated with silver and copper ores. It is commonly found in regions with significant mineralization activity, such as ore veins and hydrothermal veins. Glaucodote can often be identified based on its distinct bluish-gray color and metallic luster.
As a relatively rare mineral, glaucodote is primarily valued for its aesthetic appeal and its occurrence as a collector's mineral. Its metallic luster and unique color make it an interesting addition to mineral collections and can also be used in jewelry making as an ornamental stone. However, due to its scarcity, it does not have any significant industrial applications.
In terms of its physical properties, glaucodote has a relatively high hardness of 3.5 to 4 on the Mohs scale, making it susceptible to scratching. Its crystal structure is orthorhombic, which gives it a distinct cleavage. Glaucodote also possesses a high specific gravity, typically ranging from 5.7 to 5.8, indicating its relatively high density compared to other minerals.
Common Misspellings for GLAUCODOTE
- flaucodote
- vlaucodote
- blaucodote
- hlaucodote
- ylaucodote
- tlaucodote
- gkaucodote
- gpaucodote
- goaucodote
- glzucodote
- glsucodote
- glwucodote
- glqucodote
- glaycodote
- glahcodote
- glajcodote
- glaicodote
- gla8codote
- gla7codote
- glauxodote
